The Sveconorwegian magmatic and tectonometamorphic evolution of the high-grade Proterozoic Flekkefjord complex, South Norway.
Abstract
The Precambrian Flekkefjord complex is situated in the core zone of the Sveconorwegian orogenic belt in south-western Norway, covering the transitional zone between the south Rogaland anorthosite province to the west and the Agder migmatite terrane to the east. The Flekkefjord complex is divided into 3 suites: the banded gneiss suite, the granitic gneiss, and the post-kinematic plutonic suite. (Forkortet)